An Elastic Stress-Strain Relationship for Porous Rock Under Anisotropic Stress Conditions

被引:41
|
作者
Zhao, Yu [2 ]
Liu, Hui-Hai [1 ]
机构
[1] Univ Calif Berkeley, Lawrence Berkeley Natl Lab, Div Earth Sci, Berkeley, CA 94720 USA
[2] Chongqing Univ, Coll Civil Engn, Chongqing 630044, Peoples R China
关键词
Constitutive relationship; Coupled hydromechanical processes; Stress-dependent properties; Anisotropic stress conditions; MECHANICAL-BEHAVIOR; PRESSURE; CRACKS; SANDSTONE; MODULI;
D O I
10.1007/s00603-011-0193-y
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
A stress-strain relationship within porous rock under anisotropic stress conditions is required for modeling coupled hydromechanical processes associated with a number of practical applications. In this study, a three-dimensional stress-strain relationship is proposed for porous rock under elastic and anisotropic stress conditions. This relationship is a macroscopic-scale approximation that uses a natural-strain-based Hooke's law to describe deformation within a fraction of pores and an engineering-strain-based Hooke's law to describe deformation within the other part. This new relationship is evaluated using data from a number of uniaxial and triaxial tests published in the literature. Based on this new stress-strain relationship, we also develop constitutive relationships among stress, strain, and related stress-dependent hydraulic/mechanical properties (such as compressibility, shear modulus, and porosity). These relationships are demonstrated to be consistent with experimental observations.
引用
收藏
页码:389 / 399
页数:11
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